Characteristics of deep chlorophyll maximum in the Northeastern Mediterranean with respect to environmental conditions

1996-12-01
Ediger, D
Yılmaz, Ayşen
The vertical distribution of chlorophyll-a was recorded throughout the northern part of the Levantine Basin of the eastern Mediterranean and was related to patterns of the physical dynamics for October 1991-March 1994 period. A well developed deep chlorophyll maximum (DCM) was observed in the northern Levantine Basin (NLB), with concentrations greater than 1 mu g/L at depths ranging from 45 to 100 m on average. Chlorophyll-a concentrations ranged between 0.01 (in surface waters, Oct. 1991) and 3.07 mu g/L (in subsurface waters, March 1992). In general high concentrations of chlorophyll-a were observed in late winter. In cyclonic regions the depths of the DCM and the nutricline coincided and relatively high concentrations were observed at shallower depths at relatively high percentages of surface light. In anticyclonic regions the DCM (at low level of concentration) were located at the base of the euphotic zone and much above the nutricline. Well defined DCM feature was not prominent since at most of the stations, uniform distributions of chlorophyll-a were observed in the euphotic zone during the cooler winter conditions in 1992. The chlorophyll concentrations were significantly high in this winter when compared with those of ordinary mild winters. Because of the relatively low chlorophyll-a concentration resulting most probably low phytoplankton biomass in the basin and low input of material from the land, a thick euphotic zone forms with an average value of similar to 80 m.
JOURNAL OF MARINE SYSTEMS

Suggestions

CHARACTERISTICS OF THE MEDITERRANEAN UNDERFLOW IN THE SOUTHWESTERN BLACK-SEA CONTINENTAL-SHELF SLOPE REGION
OGUZ, T; ROZMAN, L (1991-01-01)
Hydrographic observations obtained during the period 6-13 August 1989 are used to illustrate characteristics of the dense water of the Mediterranean underflow in the southwestern Black Sea shelf/slope region. The inflowing warmer and saltier Mediterranean water is observed to spread north-northwestward of the channel-canyon axis along the bottom of the shelf. As the inflowing water crosses the shelf it becomes gradually cooler, fresher and thus less dense by mixing continually with the waters of the Cold In...
Seasonal variation of the phytoplankton composition in the northern Levantine Sea
Yücel, Nebil; Uysal, Zahit; Tuğrul, Süleyman (2017-10-13)
Seasonal and spatial distribution of phytoplankton pigment composition in July & Sep 2012 and Mar & May 2013 was studied at five stations in different parts of the northern Levantine Sea from Mersin Bay to Rhodes Gyre. Total chlorophyll a concentrations varied 0.001 – 0.578 mg m-3 during the study. The highest value was measured in cyclonic Rhodes Gyre at 70 meters in Deep Chlorophyll Maximum (DCM). But, concentrations were found less than 0.1 mg m-3 in offshore waters and Rhodes Gyre. Seven phytoplankton g...
Spatio-temporal variability of the size-fractionated primary production and chlorophyll in the Levantine Basin (northeastern Mediterranean)
Yucel, Nebil (Elsevier BV, 2018-7)
Spatial and temporal variations in size-fractionated primary production (PP) and chl a, in relation to ambient physicochemical parameters, were studied in the three distinct ecosystems of northeastern Levantine Basin namely eutrophic Mersin Bay, mesotrophic Rhodes Gyre, and oligotrophic offshore waters. These ecosystems were visited in July and September 2012 and March and May 2013. Total primary production (TPP) rates ranged between 0.22 and 17.8 mg C m(-3) h(-1) within the euphotic zone, whereas depth-int...
DISTRIBUTION OF SURFICIAL SHELF SEDIMENTS IN THE NORTHEASTERN AND SOUTHWESTERN PARTS OF THE SEA OF MARMARA - STRAIT AND CANYON REGIMES OF THE DARDANELLES AND BOSPORUS
ERGIN, M; BODUR, MN; EDIGER, V (Elsevier BV, 1991-02-01)
Surficial sediment samples collected from the northeastern and southwestern shelf regions of the Sea of Marmara, together with data available from other sources, indicate marked variations in sediment compositions resulting from differences in topographical, hydrological and biological conditions. In the strait channels of the Dardanelles and Bosporus, where strong undercurrents prevail, the floor was covered mostly by coarse-grained sediments (rich in sand and gravel). However, in areas of relatively low e...
Interannual variability of the early summer coccolithophore blooms in the Black Sea: impacts of climatic factors
Cokacar, T; Oguz, T; Kubilay, N (2003-08-06)
Interannual variability of the early summer (May-June) coccolithophore blooms within surface waters of the Black Sea was studied by means of satellite-based bio-optical observations. The performance of two coccolithophore detection algorithms were tested for Black Sea conditions, and were found to provide comparable spatial patterns consistent with the corresponding true color images. An analysis of six, year-long OCTS and SeaWiFS imagery from 1997 onwards points to the presence of a major phytoplankton blo...
Citation Formats
D. Ediger and A. Yılmaz, “Characteristics of deep chlorophyll maximum in the Northeastern Mediterranean with respect to environmental conditions,” JOURNAL OF MARINE SYSTEMS, pp. 291–303, 1996, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/63236.